Kazakh Steppe

Setting

The steppe extends more than 2,200 km (1,400 mi) from the east of the Caspian Depression and north of the Aral Sea, all the way to the Altai Mountains. It is the largest dry steppe region on earth, covering approximately 804,450 km² (310,600 sq mi). The Kazakh Steppe lies at the southern end of the Ural Mountains, the traditional dividing line between Europe and Asia. Much of the steppe is considered to be semi-desert, grading into desert as one goes further south. The Turan Lowland lies in the southwestern part of the steppe, but elevation increases as one travels east or to the northern parts of the steppe, with a few exceptions.

The Pontic Steppe lies to the west and northwest. To the north and northeast of the Kazakh Steppe lies the Kazakh forest steppe, an ecoregion of pine groves interspersed with grasslands that forms a transition between the Kazakh steppe and the forests of Siberia. To the south lies the Kazakh semi-desert and the Kazakh upland ecoregions. The Kokshetau Massif in north-central Kazakhstan harbors an enclave of the Kazakh upland, distinct from the Kazakh steppe which surrounds it at lower elevations.

Climate

The region has a semi-arid, continental climate. Most of the area falls under the cool semi-arid (BSk) classification under the Köppen climate classification system, although the moister north is classed as humid continental (Dfa/Dfb). The steppe receives between 200 and 400 millimetres (8 and 16 in) of precipitation in an average year, with more falling in the northern areas. Average maximum temperatures range from 20 to 26 °C (68.0 to 78.8 °F) in July, and from −12 to −18 °C (10.4 to −0.4 °F) in January. Very high winds sweep across the plains at times.